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Published in final edited form as: Neuroscience. 2009 Nov 6;165(3):715. doi: 10.1016/j.neuroscience.2009.11.003

Monitoring transient Ca2+ dynamics with BK channels at active zones in frog saccular hair cells

Thanh Sy 1, Alan D Grinnell 2, Arthur Peskoff 2, Bruce Yazejian 1
PMCID: PMC2814894  NIHMSID: NIHMS158674  PMID: 19897018

Abstract

Neurotransmitter release from the basolateral surface of auditory and vestibular hair cells is mediated by Ca2+ influx through voltage-gated Ca2+ channels. Co-localization of large-conductance Ca2+-activated K+ (BK) channels at the active zones of these cells affords them with an optimal location to act as reporters of the Ca2+ concentration changes at active zones of transmitter release. In this report we use BK channels to monitor dynamic changes in intracellular Ca2+ concentration during transient influxes of Ca2+, showing that BK current magnitude and delay to onset are correlated with the rate and duration of Ca2+ entry through Ca2+ channels. We also show that BK channels exhibit a much higher Ca2+ binding affinity in the open state than in the closed state.

Keywords: patch clamp, Ca2+ channels, transmitter release

Introduction

The release of neurotransmitter is triggered by a rapid rise in the intracellular free Ca2+ concentration due to the influx of Ca2+ through nerve terminal voltage gated Ca2+ channels opened by depolarization (Katz, 1969; Augustine et. al., 1987; Clapham, 2007). The spatial and temporal restriction of Ca2+ to active zones—regions near Ca2+ channels that are the sites of transmitter release—is achieved through the action of low affinity Ca2+ buffers with rapid kinetics (Zucker, 1996; Neher, 1998; Roberts, 1993, 1994; Issa and Hudspeth, 1996). Perhaps equally important—to enable repetitive signaling—is the subsequent rapid reduction of the active zone Ca2+ concentration to baseline levels following closure of the Ca2+ channels. Rapid build-up and decay of concentrations of Ca2+ high enough to trigger transmitter release are especially important for auditory and vestibular hair cells that can release transmitter at very high frequencies (Smotherman and Narins, 1999; Fettiplace and Fuchs, 1999; Glowatzki and Fuchs, 2002; Fuchs, 2005; Rutherford and Roberts, 2009). In order to track the time course of the changes in intracellular Ca2+ concentration at active zones we monitored the activity of large-conductance Ca2+-dependent K+ (BK) channels in frog saccular hair cells that co-localize at active zones with Ca2+ channels (Roberts, et. al., 1990; Issa and Hudspeth, 1994; Armstrong and Roberts, 1998, 2001). Ca2+-activated channels have previously been used to estimate the intracellular Ca2+ concentration in a number of preparations (Roberts et al., 1990; Tucker and Fettiplace, 1996; Prakriya and Lingle, 2000; Yazejian et al., 2000). In this report we use BK channels to track intracellular Ca2+ concentration changes that result from transient fluxes of Ca2+ through Ca2+ channels. We show that the time to onset and extent of activation of BK channels depend upon the rate and duration of Ca2+ entry. The slow rate of BK channel deactivation—at depolarized voltages where Ca2+ influx is terminated—reflects either the intrinsic kinetics of BK channel closure or the much greater Ca2+ binding affinity of channels in the open state.

Experimental procedures

Cell isolation

All animals used in this study were handled in compliance with the policies and procedures of the Animal Care and Use Committee at Mt. St. Mary’s College and with the National Institute of Health Guide for the Care and Use of Laboratory Animals (NIH Publications No. 80–23). Hair cells were isolated from the sacculus of the grass frog (Rana pipiens) as described previously (Hudspeth and Lewis, 1988). Sacculi were dissected free from the labyrinth and immersed in a low Ca2+ solution (LoCaS) of the following composition: 100 mM NaCl, 2 mM KCl, 50 μM CaCl2, 50 μM MgCl2, 3 mM glucose, 30 mM HEPES, pH 7.3, supplemented with cysteine-activated papain (0.5 mg/ml L-cysteine + 0.5 mg/ml papain (Calbiochem 5125)). After 30–60 minutes in papain, sacculi were moved to fresh LoCaS supplemented with 1 mg/ml BSA for 60 minutes. Sacculi were then transferred to a recording dish containing frog Ringer of the following composition: 116 mM NaCl, 2 mM KCl, 1 mM CaCl2, 1 mM 3,4 diaminopyridine (DAP) and 5 mM HEPES, pH 7.3. The Ringer solution was supplemented with 10 nM of the specific BK channel blocker paxilline (Sanchez and McManus, 1996). This was done to reduce the magnitude of the BK currents to allow for adequate voltage control. A dog hair (Weimaraner) was used to scrape off the cells from the epithelium.

Electrophysiology

Patch electrodes were fabricated from borosilicate glass (Sutter BF 150-86) using a two-stage puller (Narishige PP-97) to yield tip diameters of about 1 μm with an electrode resistance (with our internal solutions, see below) of 3–5 MΩ. To record BK currents, pipettes were filled with a quasi-internal solution of the following composition: 52 mM K2SO4, 38 mM KCl, 1 mM K-EGTA, 1 mM DAP and 5 mM HEPES pH 7.3, supplemented with 200–300 μg/ml amphotericin-B. To record Ca2+ currents, the pipettes were filled with a solution of the following composition: 52 mM CsMeSO4, 38 mM CsCl, 1 mM EGTA, 1 mM DAP, 50 mM D-glucose, 5 mM HEPES, pH 7.3 and amphotericin-B as above. For Ca2+ current recordings the bath solution was switched to one of the following composition: 116 mM NaCl, 2 mM KCl, 2 mM CaCl2, 10 mM TEACl, 1 mM 3,4 diaminopyridine (DAP), 1 μM paxilline and 5 mM HEPES, pH 7.3. Perforated patch recordings (Horn and Marty, 1988; Rae et al., 1991) were performed using a MultiClamp 700B patch-clamp amplifier in combination with a Digidata 1440A analog-to-digital interface (Molecular Dynamics, Foster City, CA). Pulse paradigms and data analysis were performed with the pCLAMP 10 suite of software programs (Molecular Dynamics). Currents were acquired at 50 kHz and filtered at 10 kHz. Series resistance (typically 8–15 M Ω) was compensated 85–95% and linear leak and capacitive currents were subtracted using a P/-8 protocol (Bezanilla and Armstrong, 1977). Experiments were performed at room temperature (22–24°C). Figures were made with the Origin 7.5 graphing software package (Microcal).

Results

BK channel activation with different rates and durations of Ca2+ entry

Figure 1 shows results from an experiment designed to monitor the build-up and decay of intracellular Ca2+ as a function of the rate and duration of Ca2+ entry using BK currents as a measure of submembrane [Ca2+]. Voltage pulse paradigms are shown above each set of records with the intermediate potentials (IPs) indicated (see below). For these experiments the membrane voltage was initially stepped from a holding potential of −70 mV to +130 mV (above the Ca2+ equilibrium potential) for 10 msec to maximize the opening of voltage-gated Ca2+ channels while minimizing the Ca2+ driving force. Thus, at +130 mV a maximum number of Ca2+ channels opened but no Ca2+ influx occurred. After this initial step, the voltage was repolarized to IPs of +130 mV (i.e. no step change), +50 mV, +10 mV, −30 mV or −70 mV for durations of 100 μsec, 300 μsec, 500 μsec, 1 msec, 3 msec and 5 msec before returning to +130 mV for an additional 80 msec.

Figure 1.

Figure 1

BK currents activated in response to different rates and durations of Ca2+ influx. Current records in this and all figures are the average of three presentations of the voltage waveform. Stimulus waveforms are given above each set of traces—most clearly delineated in F. In all records the membrane potential was first stepped from a holding potential of −70 mV to +130 mV for 5 msec to open Ca2+ channels but not allow Ca2+ entry. The potential was then transiently stepped to intermediate potentials of +50 mV, +10 mV, −30 mV or −70 mV for 100 μsec, 300 μsec, 500 μsec, 1 msec, 3 msec or 5 msec to allow Ca2+ entry before re-depolarization to +130 mV to stop Ca2+ influx. A-F: Current responses to various times and intermediate potential voltages. The dotted line in each record shows the response to a step to +130 mV only (i.e. no intermediate voltage step). Inset a shows—in a different cell—the progressive block of BK current in response to application of 100 nM paxilline. Voltage presentations were given at 5 sec intervals: IP was −50 mV, 3 msec; scale bars 2 nA, 10 msec. Inset b—also from a different cell—shows the current responses to test pulses of +130 mV (dotted line) and +50 mV (solid line) after IP steps to +10 mV. Scale bars are the same as in inset a.

During the IP steps Ca2+ entry occurred independent of Ca2+ channel opening kinetics (Hudspeth and Lewis, 1988) and continued as long as the Ca2+ channels remained open. Furthermore, the rate of Ca2+ entry was dependent on the Ca2+ driving force at each IP. The IP steps generated a mixed current of Ca2+ flowing through already opened Ca2+ channels and BK channel current flowing in response to the rise in the free Ca2+ concentration resulting from the Ca2+ influx. Subsequent re-depolarizations to +130 mV then generated currents that largely flowed through BK channels as Ca2+ entry was terminated and the driving force for BK channel current was increased. Thus, the evoked BK currents measured during the second step to +130 mV should reflect the [Ca2+] present near the BK channels just prior to and during the step depolarization. For very short duration IPs, where few BK channels have opened, the subsequent step to +130 mV generated a BK current flowing mostly through channels that opened due to this step change of voltage, but were not open during the IP. On the other hand, after longer times spent at the IP the BK current seen at +130 mV predominately flowed through channels that had opened at the IP and were suddenly subjected to a larger K+ driving force. As the BK channels might be expected to close at a rate consistent with the decline of the free Ca2+ concentration, the duration of the BK current at +130 mV (where Ca2+ influx ceases) may potentially be a measure of the duration of a concentration of free Ca2+ sufficient to maintain BK channel opening.

Figure 1A shows that, superimposed on a Ca2+-independent outward current in response to the initial +130 mV step, a 100 μsec IP step to either −70 mV or −30 mV led to the generation of an additional outward current during the second step to +130 mV (solid black and green traces respectively). As these outward currents occurred only after the IP steps (compare with the dotted line showing the current in response to a step to +130 mV only), they are consistent with their being BK currents flowing in response to the Ca2+ influx during the IP. In fact, these outward currents were blocked by application of 100 nM of the BK channel blocker paxilline (Sanchez and McManus, 1996) (see inset a of Figure 1). At an IP duration of 100 μsec, the largest BK current evoked at +130 mV was seen in response to the IP of −70 mV. With longer durations at the IP of −70 mV the magnitude of the BK current generated during the second +130 mV step increased, reached a maximum with an IP step duration of 300 μsec, and then declined in peak magnitude as the potential was held at this IP for longer and longer times (compare the black traces in Figure 1 A-F). By comparison, at an IP step of +50 mV (red traces) there was no BK current generated during the +130 mV step that followed the 100 μsec IP step (red trace in Figure 1A) and only a very small current was seen with a 300 μsec step (when the step to −70 mV yielded the largest current for that IP). However, longer durations at +50 mV led to larger and larger BK currents, becoming maximal at 5 msec IP duration (Figure 1F).

At −70 mV, where the Ca2+ driving force would be the greatest, one would expect the greatest rate of Ca2+ entry. On the other hand, at this potential Ca2+ channels close rapidly leading to a decline in the Ca2+ influx and a limit to the free Ca2+ concentration near the BK channels. In contrast, at +50 mV one would expect a slower but continuous Ca2+ influx due to the lower Ca2+ driving force and maintained channel opening. These features of the expected Ca2+ influx are observed with the BK current behavior as measured at +130 mV. That is, for the IP of −70 mV, the BK current turned on with short durations of Ca2+ entry (e.g. the first 100 μsec of the tail current) and diminished rapidly as the potential was maintained at −70 mV before stepping to +130 mV. Likewise, the BK current measured at +130 mV in response to the IP step of +50 mV built up slowly but didn’t diminish in magnitude for long IP durations (e.g. 5 msec).

Figure 2 summarizes results from several experiments like that of Figure 1. Plotted are the normalized BK peak current magnitudes measured at +130 mV as a function of the time spent at different IPs. Note that the peak magnitudes of the responses are plotted here and not the time courses of the responses themselves. As was seen in Figure 1, the peak current magnitude measured after the IP steps to −70 mV increased most quickly (requiring the shortest duration of Ca2+ entry), and fell most quickly, being back to baseline by 2 msec of IP duration. Similar phasic responses in the magnitude of the BK currents were seen with IPs of −50 mV and −30 mV (and to a lesser extent, −10 mV) but in these cases the maximum BK magnitudes obtained were larger, the peak responses required longer IP durations, and the BK current magnitudes fell more slowly. The BK current magnitude responses to IPs between +10 mV and +50 mV were slower still in reaching their peak values and did not decline for longer IP durations. The plot of the responses to the IP of +70 mV was the slowest of all: even 3 msec of Ca2+ entry at this potential was insufficient to activate all of the BK channels that could be activated by the 3 msec steps to IPs between +10 mV and +50 mV.

Figure 2.

Figure 2

Summary data of normalized peak BK current measured at +130 mV vs. time spent at each of the intermediate potentials. Each symbol represents an average of six experiments like that of Figure 1. Error bars represent ±SD.

Correlation of Ca2+ currents with BK channel activation

To understand the relationship between the magnitude and rate of Ca2+ entry during the IP steps and the subsequent BK currents measured at +130 mV, we recorded Ca2+ currents in response to the same waveforms as presented in Figure 1. Figure 3 shows these measured Ca2+ currents (continuous traces, inverted for clarity) in response to steps from +130 mV to the IPs of −70 mV, −10 mV and +50 mV. Superimposed on these Ca2+ currents are the corresponding normalized BK current magnitudes measured during steps to +130 mV after different durations at these IPs (as in Figure 2).

Figure 3.

Figure 3

Correlation of BK current magnitude measured at +130 mV with Ca2+ influx at three intermediate potentials. Continuous traces are Ca2+ currents (inverted for clarity) measured at the indicated potentials after a step from +130 mV (voltage steps not shown). Symbols are average peak normalized BK currents measured at +130 mV (taken from Figure 2) after different durations at the IPs. Ca2+ currents and BK currents were measured in different cells. The inset shows the relationship between the Ca2+ current and voltage for steps from +130 mV.

The Ca2+ tail current recorded in response to a step from +130 mV to −70 mV (left panel) peaked in magnitude in less than 300 μsec and was over in less than 1 msec. The BK current magnitude responding to a +130 mV step given at different times during the tail current peaked slightly later than the peak of the Ca2+ current and declined with a delay, persisting for about 1 msec after the cessation of the Ca2+ influx. The middle panel shows the Ca2+ current measured during a step from +130 mV to −10 mV and the BK responses (again, measured at +130 mV) at various times during this IP step. Here the Ca2+ current was slower to rise and the peak smaller than at −70 mV, but the influx declined only slightly, persisting throughout the 3 msec step. The BK current magnitudes associated with fractions of this Ca2+ current rose more slowly (than the current magnitudes in response to the steps to −70 mV) but reached a larger peak value before declining slightly. Finally, the Ca2+ current recorded in response to the step to +50 mV had the slowest rate of rise and the smallest peak value. Unlike the other two, it did not decline after reaching its peak value. The BK currents for this IP also rose in magnitude more slowly but—unlike the responses to −70 mV—and −10 mV steadily increased in response to increasing fractions of the Ca2+ influx during the 3 msec step.

The slow influx of Ca2+ during the step to +50 mV led to an accumulation of intracellular Ca2+ that was able to open as many BK channels as the rapid Ca2+ influx at −10 mV but required more Ca2+ influx time. On the other hand, because of the brief influx of Ca2+ at −70 mV, only about half as many BK channels were activated as could be activated with IP steps to −10 mV and +50 mV. The correlation of the rate of rise and fall of the magnitude of the BK current in response to different rates and durations of Ca2+ entry suggests that BK channels were closely monitoring the Ca2+ concentration changes that were occurring during these voltage steps and gives an indication of the speed with which the Ca2+ concentration rose above threshold for activation of BK channels.

BK channel deactivation after exposure to high [Ca2+]

The results from Figure 1 suggest that, for each trace, the decline of the BK current during the maintained +130 mV step reflects the rate of disappearance of a Ca2+ concentration sufficient to maintain BK channels in an open configuration. This follows from the presumption that, as the potential approaches +130 mV, the Ca2+ influx should stop and that any persistent BK channel conductance should be a result of lingering free Ca2+ near the BK channels. Note that this decline in the BK current is deactivation, not inactivation. The evidence for this is twofold. First, as reported by Armstrong and Roberts, 1998, 2001) the inactivation of BK channels in frog saccular hair cells is removed by papain. Our cell isolation procedure includes this enzyme treatment (see Experimental Procedures). Second, as shown in inset b of Figure 1, the BK current was maintained (i.e. did not inactivate) when the test potential given after the IP step was below ECa2+ where Ca2+ influx continued. It is unclear however, whether the decline in the BK currents themselves at +130 mV (as opposed to the decline in their maximum elicitable magnitudes) was due primarily to the decline in the ambient [Ca2+] near them or to the kinetics of deactivation of the BK channels.

To distinguish between these possibilities we performed the experiments of Figure 4. Figures 4A and 4B show results from experiments where the membrane potential was stepped to an IP of either +10 mV or −30 mV for 5 msec before testing the BK current response at +130 mV (similar to the experiments illustrated in Figure 1F). However, (unlike the experiments of Figure 1F), after 5 msec at +130 mV, the potential was transiently repolarized to −70 mV for different lengths of time before returning to +130 mV for an additional 80 msec. Stepping to −70 mV should have two effects. First, it should lead to the deactivation of BK channels and second it should close the Ca2+ channels and stop the entry of Ca2+ (after allowing a transient Ca2+ influx from the tail current). Upon return to +130 mV, BK channels should re-open depending on the available Ca2+ (including residual Ca2+ from the IP step and the additional Ca2+ from the tail current).

Figure 4.

Figure 4

Deactivation of BK currents. Stimulus waveforms are presented above each set of currents records. In A and B, a step to +130 mV was followed with an intermediate step to +10 and −30 mV respectively followed by a second depolarization to +130 mV (as in Figure 1). The second +130 mV step was interrupted after 5 msec by steps to −70 mV for 0 msec (i.e. no step to −70 mV), 0.5 msec, 1.0 msec, 1.5 msec, 2.0 msec, 2.5 msec, or 3.0 msec before a third depolarization to +130 mV. In C and D, after an intermediate step to +10 mV and −30 mV respectively, a second depolarization to +130 mV was given except that it was preceded by steps to −70 mV for the same times as in A and B. For all records the dotted line represents the current response to a step to +130 mV only.

Consider first the responses to the IP of +10 mV (Figure 4A). The solid black trace indicates the control response to a waveform where the second step to +130 mV was uninterrupted (i.e. no step to −70 mV). A short sojourn to −70 mV (0.5 msec—red trace) led to a BK current at +130 mV that reached nearly the same magnitude as the current in the uninterrupted trace and that declined at a similar rate. However, after longer times spent at −70 mV before return to +130 mV (e.g. 1 msec-blue trace) the peak BK current evoked was less than the current at that time in the uninterrupted pulse. Evidently the BK channels that closed during the 1 msec step to −70 mV did not reopen upon re-depolarization to +130 mV to the level of the black trace (i.e. no step to −70 mV) even though the Ca2+ concentration near the BK channels at that time during the +130 mV step was likely to have been no lower than it would have been had the step to −70 mV not been made. In fact there was probably more Ca2+ due to the influx of Ca2+ during the tail current. Holding the potential at −70 mV for increasingly longer times (greater than 1.5 – 2.0 msec) exceeded the time of the Ca2+ tail current (cf. Figure 3). As a result, the subsequent steps to +130 mV generated no BK current since after these long sojourns at −70 mV there was evidently not enough Ca2+ to re-open them.

Figure 4B shows the results from a similar experiment but where the IP step was to −30 mV instead of +10 mV. Note that—in contrast to the result with a +10 mV IP—the 0.5 msec sojourn to −70 mV after the IP step (red trace) led to a larger BK current at +130mV than was seen without the interruption—likely due to the re-opening of BK channels due to the Ca2+ tail current. As with the paradigm with the +10 mV IP step, longer interruptions of the +130 mV step to −70 mV led to rapid closure of the open BK channels that could not be re-opened by the step back to +130 mV. In both cases (the IPs of +10 mV and −30 mV) the BK channels that would have remained open at +130 mV were unable to re-open if they were closed with a prolonged step to −70 mV.

Another set of experiments designed to test the BK channel’s ability to track the Ca2+ concentration changes at the active zone is illustrated by the results in the bottom panel of Figure 4. In these experiments Ca2+ entry was terminated (save for a Ca2+ tail current) and BK and Ca2+ channels were closed following 5 msec steps to +10 mV or −30 mV by stepping to −70 mV for various times before testing the BK channel status at +130 mV. Immediate steps to +130 mV from the IPs (i.e. no step to −70 mV first) generated BK currents consistent with the amount of Ca2+ likely to have been available at the time of the step up (black traces). Thus, the BK current was larger for the step from the IP of +10 mV than from −30 mV. In both cases, steps to −70 mV even as short as 0.5 msec (red traces) led to the generation of BK currents at +130 mV that were smaller than they were without the step to −70 mV. Evidently, by stepping to −70 mV, many of the BK channels that were open during the IPs closed and were not able to be reopened upon being stepped to +130 mV even though the −70 mV—step would have introduced more Ca2+. Longer durations (greater than 0.5 msec) spent at −70 mV further closed the BK channels leading to a decline in the BK current magnitude measured at +130 mV.

Discussion

BK channels are well positioned to report the Ca2+ concentration changes that occur during and after Ca2+ entry through Ca2+ channels. The spacing of intramembraneous particles thought to be Ca2+ and BK channels in freeze-fracture replicas of these active zones (Roberts et al., 1990) suggests that the BK channels are on the order of 10 nm away from Ca2+ channels. A more recent report estimated the distance between rat brain Ca2+ and BK channels to be ~10–15 nm (Berkefeld et al., 2006). These authors, using affinity purification techniques, showed that BK channels co-isolate into macromolecular complexes with voltage gated Ca2+ channels. Further evidence for the close association of BK and Ca2+ channels is provided by the finding that millimolar concentrations of the Ca2+ chelator BAPTA can intercept the Ca2+ entering through voltage-gated channels to prevent BK channel activation while the slower Ca2+ buffer EGTA is ineffective (Roberts, et. al., 1990; Prakriya and Lingle, 2000; Berkefeld et al., 2006). These results are consistent with the differential effects of these buffers on transmitter release (Adler et al., 1991; Augustine et. al., 2003) suggesting that BK channels are at a similar distance from the Ca2+ channels as are the Ca2+ sensors in the release apparatus.

BK channels monitor the rate and duration of Ca2+ entry

We find that the rate and duration of Ca2+ entry through Ca2+ channels are correlated with the time to onset and magnitude of BK currents. The profile of intracellular Ca2+ concentration changes near Ca2+ channels seems to be what the BK channels report. Rapid but brief rates of Ca2+ entry at potentials with large Ca2+ driving forces but where Ca2+ channels tend to close (e.g. −70 mV, Figure 3) yield BK currents with the shortest delay to onset—consistent with locally higher Ca2+ concentrations. On the other hand, slower, continuous Ca2+ entry at higher potentials (e.g. +50 mV, Figure 3) activates more BK channels but only after a longer delay to onset—consistent with a lower concentration of Ca2+ reaching a greater number of BK channels. The maximum BK current measured in response to continued, slow Ca2+ influx rates required longer times than were needed with larger Ca2+ driving forces.

BK channels deactivate slowly at depolarized levels after exposure to high Ca2+

Our results suggest that the slow decline in the BK current measured at +130 mV following steps to IPs that allow Ca2+ influx is either due to the rate of decline of the free Ca2+ in the vicinity of the BK channels or is a result of the rate of deactivation of the channels in the absence of an increased Ca2+ concentration.

We used two methods to shut off Ca2+ entry—by going to ECa (stepping to +130 mV) or by closing the Ca2+ channels (stepping to −70 mV). These two methods have different effects on the BK channels. By stepping to +130 mV the BK channels—while being deprived of continuous Ca2+ influx—will still be depolarized. At this potential some channels remain open for tens of msec. Apparently, BK channels are slow to deactivate at depolarized voltages if they have previously been exposed to a high enough Ca2+ concentration to open them. This is true even if the ambient Ca2+ concentration falls to a level that will not allow them to open de novo. This finding supports the conclusions of Cox and Aldrich (2000) that the BK channel’s affinity for Ca2+ is higher when the channel is open than when it is closed. In our preparation the BK channels may be remaining open for prolonged periods of time after cessation of Ca2+ entry at +130 mV because they are binding more tightly the Ca2+ that opened them. On the other hand, some of the BK channels that do close at +130 mV can remain sensitive to Ca2+ and can re-open if exposed to a high enough [Ca2+] (as can be provided for example by a Ca2+ tail current—Figure 4B).

The second method we used to stop Ca2+ entry—stepping to −70 mV to close the Ca2+ channels—also repolarizes the BK channels. Hair cell BK channels close quickly at −70 mV—the tail current decays exponentially with a time constant of 1.0 ms at −70 mV (Hudspeth and Lewis, 1988). We find that BK channels cannot be reopened upon redepolarization from prolonged stays at −70 mV (Figures 4C and 4D). The implication from this finding is that opening the channels requires a higher concentration of Ca2+ than is needed to keep them open. Our results provide an upper limit of ~2.0 msec to the time that the [Ca2+] remains above threshold to open BK channels after the cessation of Ca2+ entry. This conclusion stems from the finding that BK currents are unactivatable by a large depolarizing step given 2.0 msec after the peak of a Ca2+ tail current (Figures 3 and 4).

The present report demonstrates that the rate of activation and delay to onset of BK channels reflect the dynamic changes in intracellular Ca2+ concentration close to Ca2+ channels during and after the transient influx of Ca2+.

Acknowledgments

Grants

This work was supported by the National Science Foundation Research in Undergraduate Institutions Grant #0854551 to B. Yazejian and a National Institutes of Health Minority Access to Research Careers Grant (5T34GM008415-18) to the Biology Department at Mount St. Mary’s College.

Footnotes

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